RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES3002, doi:10.2205/2017ES000598, 2017
Figure 12. The distribution of focal earthquake mechanisms and fault discontinuities at the Mohns Ridge (the bathymetric base is SRTM-30 v.5). I–IV are the main blocks of the Mohns Ridge; F1–F8 are faults as tentatively identified here. Lines 1–6 mark the seafloor relief inhomogeneities discussed here.
Citation: Usenko S. V., A. N. Boyko, T. V. Prokhorova (2017), Seafloor relief inhomogeneities and the tectonics of the Greenland-Lofoten Basin in the North Atlantic, Russ. J. Earth Sci., 17, ES3002, doi:10.2205/2017ES000598.
Copyright 2017 by the Geophysical Center RAS.
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